RT Journal Article
T1 Drenaje fluvial y topografía ligados a extensión: NÈ dé Iberia
T1 Fluvial drainage and topography related to extension: NE of Iberia
A1 Vergés i Masip, Jaume
A1 Lewis, C.
A1 Marzo, M.
AB Integrated analysis of fluvial drainage pattern, digital topography and regional tectonics allows to determine the lateral extent of high topography linked to the extensional system of faults that parallels the coastline of the northeastern Iberia. The development and rise of the present morphotectonic units of Sierra Prelitoral (upper Oligocene-Lower Miocène) and Sierras Transversales (upper Miocene to present) as rift flarik processes, reorganized the previous fluvial drainage system and originated thé present one.The Sierra Prelitoral bounds the NE-SW trend of faults that limit the El Camp and Vallès-Penedès grabens whereas the Sierras Tansversals bound the NNW-SSE trend of faults related to the Empordà graben system. The different relative positions of external normal fault, maximum local relief and water divide in the Sierras Tansversals support the idea of very young topography related to active normal faulting
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12464
UL http://hdl.handle.net/10272/12464
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026